Assessment of Wildfire Susceptibility and Wildfire Threats to Ecological Environment and Urban Development Based on GIS and Multi-Source Data: A Case Study of Guilin, China
Abstract
:1. Introduction
2. Study Area and Data Overview
2.1. Study Area
2.2. Historical Wildfire Dataset
2.3. Susceptibility Conditioning Factors
2.4. Ecological and Urban Vulnerability Factors
2.4.1. Ecological Vulnerability Factors
2.4.2. Urban Vulnerability Factor
3. Methods
3.1. Multicollinearity Test
3.2. Wildfire Susceptibility Modeling Based on Machine Learning
3.2.1. Logistic Regression (LR)
3.2.2. Artificial Neural Network (ANN)
3.2.3. K-Nearest Neighbor (KNN)
3.2.4. Support Vector Regression (SVR)
3.2.5. Random Forest (RF)
3.2.6. Gradient Boosting Decision Tree (GBDT)
3.2.7. Light Gradient Boosting Machine (LGBM)
3.2.8. eXtreme Gradient Boosting (XGBoost)
3.3. Performance Assessment of Susceptibility Models
3.4. SHapley Additive exPlanations (SHAP) Method
3.5. Ecological and Urban Vulnerability Modeling
3.6. Wildfire Risk Modeling
4. Results
4.1. Wildfire Susceptibility Assessment
4.1.1. Multicollinearity Test Results
4.1.2. Wildfire Susceptibility Map
4.1.3. Model Performance Assessment
4.1.4. Results of SHAP Method
- (1)
- Temperature positively influences the occurrence of wildfires, as higher temperatures result in larger Shapley values and a greater likelihood of wildfire outbreaks. When the temperature exceeds 17.3 °C, the Shapley value is generally greater than 0, indicating higher susceptibility to wildfire disasters.
- (2)
- Except for FLc, LXf, RGc, RGd, RK, and WR soil types, all other soil types have the potential to experience wildfires. Among them, soil types such as Ach and Acf generally have a Shapley value greater than 0, making them more susceptible to wildfire disasters.
- (3)
- Compared to cropland and forest, samples belonging to grassland have the highest Shapley value, making them more susceptible to wildfire disasters.
- (4)
- Overall, the Shapley value of samples increases with an increase in the distance to roads. When the distance to roads is greater than 500 m, the Shapley value is greater than 0, indicating that wildfire disasters in Guilin are more likely to occur in areas far from human activity.
- (5)
- When slope is within the range of [5°, 25°], the Shapley value is greater than 0, indicating a positive effect on the occurrence of wildfires. The mountains within this range of inclination tend to receive more direct sunlight and are more exposed to natural winds, thus causing vegetation to dry out faster and become more combustible.
- (6)
- When wind speed is in the interval of [0 m/s, 0.6 m/s], the Shapley value decreases with the increase in the wind speed, while when the wind speed is greater than 0.6 m/s, the wind speed has a positive impact on the occurrence of wildfires, and the Shapley value of the sample increases with the increase in the wind speed. Moreover, when the wind speed is greater than 0.8 m/s, the Shapley value is generally greater than 0, indicating a higher probability of wildfire disasters.
- (7)
- When the distance to rivers is in the range of (0, 1000 m), the Shapley value of the sample gradually increases and is greater than 0; however, when the distance to rivers is greater than 1000 m, the Shapley value of the sample shows a downward trend, indicating that the area near the river is more prone to wildfire disasters.
- (8)
- There is a non-monotonic relationship between elevation and wildfire. The samples with Shapley value greater than 0 are basically located in the range of (250 m, 1000 m), and the probability of wildfires is high; when the elevation is greater than 1000 m, the possibility of wildfires is reduced.
- (9)
- FVC exerts a positive influence on wildfire occurrence overall. When FVC is in the range of (0.6, 0.8), the Shapley value is greater than 0, and the probability of a wildfire disaster is greater.
- (1)
- For wildfire case 1, soil type, temperature, wind speed, and land use have a significant positive effect, while slope, distance to rivers, distance to urban areas, and elevation have a minor positive effect. Distance to roads has a significant negative effect, and the remaining eight factors contribute a positive effect of 0.05. The final predicted wildfire susceptibility value is 1.018, and it is classified as a wildfire.
- (2)
- For wildfire case 2, soil type, temperature, land use, and slope have a significant positive effect, while solar radiation, FVC, distance to urban areas, and distance to rivers have a minor positive effect. Distance to roads has a significant negative effect, and the remaining eight factors contribute a positive effect of 0.11. The final predicted wildfire susceptibility value is 1.051, and it is classified as a wildfire.
- (3)
- For wildfire case 3, soil type, temperature, wind speed, and land use have a significant positive effect, while slope, elevation, SPI, and distance to urban areas have a minor positive effect. Distance to roads has a significant negative effect, and the remaining eight factors contribute a positive effect of 0.04. The final predicted wildfire susceptibility value is 0.969, and it is classified as a wildfire.
4.2. Wildfire Vulnerability Assessment Considering Ecology and City
4.3. Wildfire Risk Assessment
5. Discussion
5.1. Influence of Sample Confidence on Susceptibility Modeling Results
5.2. Comparison of ML Algorithms and Importance of Conditioning Factors
5.3. Comparison of SHAP Results between the Different Machine Learning Methods
5.4. Assessment Results of Wildfires in Each District and County
6. Conclusions
- (1)
- The ensemble models demonstrated superior predictive accuracy compared to traditional machine learning models. The XGBoost model achieved an AUC of 0.927 and accuracy of 0.863. High-susceptibility areas were found to be distributed in the central, northeast, south, and southwest regions of the study area, covering 41.758% of the entire region and encompassing 74.021% of wildfire samples. This model achieved the most reasonable susceptibility zoning results and the best predictive performance, making it the optimal model.
- (2)
- By using SHAP to interpret the results of the optimal model, the impact and intensity of each factor on wildfire occurrence in the study area were identified. The effects of changes in each factor on wildfire occurrence in the region were also explored. The factors that contributed the most to wildfire occurrence were found to be temperature, soil type, land use, distance to roads, slope, wind speed, distance to rivers, elevation, and FVC.
- (3)
- The ecological environment in the south, west, and northeast of Guilin was found to be vulnerable, while the urban development of Xiufeng, Diecai, Xiangshan, and Qixing districts and their surrounding counties was also found to be vulnerable. Furthermore, the vulnerability model that comprehensively considered ecology and urban development covered more high-vulnerability areas, more accurately divided low-vulnerability and high-vulnerability areas and provided richer detailed information.
- (4)
- From the perspectives of both ecological environment and urban development, potential wildfire risk areas can be identified and evaluated in a more targeted manner. However, a comprehensive evaluation that considers both aspects can provide a more holistic assessment of the wildfire disasters risk to human survival and environmental damage. This approach can enhance the comprehensiveness and accuracy of wildfire risk assessment and serve as a scientific basis for wildfire prevention and control.
Author Contributions
Funding
Data Availability Statement
Conflicts of Interest
References
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Category | Factors | Source of Data | Format and Scale/Resolution | Data Type |
---|---|---|---|---|
Topographical | Elevation | SRTM DEM | 30 m (.tiff) | Numerical |
Slope | Numerical | |||
Aspect | Categorical | |||
Curvature | Numerical | |||
TWI | Numerical | |||
SPI | Numerical | |||
Surface environmental | FVC | Landsat 8 OLI (2013–2022) | 30 m (.tiff) | Numerical |
Soil type | Harmonized World Soil Database (HWSD) | 5′ (.tiff) | Categorical | |
Distance to rivers | National Catalogue Service for Geographic Information (in Chinese) | 1:250,000 (.shp) | Numerical | |
Anthropological | Distance to roads | National Catalogue Service for Geographic Information (in Chinese) | 1:250,000 (.shp) | Numerical |
Distance to urban areas | Numerical | |||
Land use | GlobeLand30 V2020 data (in Chinese) | 30 m (.tiff) | Categorical | |
Population density | WorldPop dataset | 1 km (.tiff) | Numerical | |
Meteorological | Rainfall (surface) | ERA5-Land reanalysis dataset (2013–2022) | 11,132 m (.tiff) | Numerical |
Solar radiation (surface) | Numerical | |||
Temperature (2 m) | Numerical | |||
Wind speed (10 m) | Numerical |
Algorithm | Hyperparameters | Value |
---|---|---|
LR | max_iter (The maximum number of iterations) | 500 |
ANN | units (the number of hidden layers activation) | 9 |
“relu” and “sigmoid” | ||
learning_rate | 0.001 | |
KNN | n_neighbors | 15 |
weights | “distance” | |
SVR | kernel function | “rbf” |
C | 4 | |
gamma | 0.06 | |
RF | max_features | 8 |
n_estimators | 500 | |
max_depth | 10 | |
GBDT | n_estimators | 240 |
max_depth | 9 | |
subsample | 0.9 | |
LGBM | n_estimators | 400 |
max_depth | 12 | |
num_leaves | 90 | |
min_child_samples | 3 | |
colsample_bytree | 0.6 | |
XGBoost | n_estimators | 600 |
max_depth | 10 | |
subsample | 0.9 | |
min_child_weight | 3 | |
colsample_bytree | 0.6 |
Conditioning Factor | Multicollinearity Scores | |
---|---|---|
TOL | VIF | |
Elevation | 0.304 | 3.287 |
Slope | 0.348 | 2.878 |
Aspect | 0.987 | 1.013 |
Curvature | 0.845 | 1.184 |
TWI | 0.419 | 2.389 |
SPI | 0.462 | 2.164 |
Land use | 0.801 | 1.248 |
Soil type | 0.900 | 1.111 |
Population density | 0.826 | 1.211 |
Distance to rivers | 0.909 | 1.101 |
Distance to roads | 0.852 | 1.174 |
Distance to urbans | 0.578 | 1.731 |
FVC | 0.696 | 1.437 |
Rainfall | 0.799 | 1.252 |
Solar radiation | 0.714 | 1.400 |
Temperature | 0.337 | 2.964 |
Wind speed | 0.641 | 1.560 |
Model | Sensitivity | Specificity | Precision | F1-Score | Accuracy | RMSE (All) | RMSE (1) | RMSE (0) |
---|---|---|---|---|---|---|---|---|
LR | 0.723 | 0.746 | 0.739 | 0.731 | 0.735 | 0.423 | 0.435 | 0.409 |
ANN | 0.737 | 0.891 | 0.870 | 0.798 | 0.814 | 0.372 | 0.423 | 0.313 |
KNN | 0.761 | 0.853 | 0.837 | 0.797 | 0.807 | 0.369 | 0.379 | 0.360 |
SVM | 0.758 | 0.883 | 0.866 | 0.809 | 0.821 | 0.372 | 0.426 | 0.310 |
RF | 0.788 | 0.917 | 0.904 | 0.842 | 0.853 | 0.335 | 0.363 | 0.305 |
GBDT | 0.814 | 0.891 | 0.881 | 0.846 | 0.853 | 0.333 | 0.359 | 0.305 |
LGBM | 0.818 | 0.899 | 0.890 | 0.852 | 0.859 | 0.330 | 0.358 | 0.301 |
XGBoost | 0.818 | 0.907 | 0.898 | 0.856 | 0.863 | 0.327 | 0.356 | 0.294 |
No. | Wildfire Disaster Site | Time | Longitude/° | Latitude/° |
---|---|---|---|---|
1 | Yijia Village, Rongjiang Town, Xing’an County | 2022.10.17 Day | 110.44891 | 25.4925 |
2 | Baimao Village, Wenqiao Town, Quanzhou County | 2022.10.17 Day | 111.08272 | 26.19362 |
3 | Yaoshan, Diecai District | 2019.12.6 Night | 110.368469 | 25.303186 |
District and County | Susceptibility Value | Susceptibility Ranking | Vulnerability Value | Vulnerability Ranking | Risk Value | Risk Ranking |
---|---|---|---|---|---|---|
Xiufeng | 0.199 | 17 | 0.493 | 1 | 0.098 | 16 |
Diecai | 0.451 | 9 | 0.461 | 4 | 0.196 | 8 |
Xiangshan | 0.377 | 12 | 0.463 | 3 | 0.171 | 11 |
Qixing | 0.300 | 15 | 0.481 | 2 | 0.138 | 14 |
Yanshan | 0.361 | 13 | 0.415 | 7 | 0.151 | 13 |
Lingui | 0.521 | 7 | 0.419 | 6 | 0.219 | 3 |
Yangshuo | 0.442 | 10 | 0.407 | 8 | 0.181 | 10 |
Lingchuan | 0.622 | 3 | 0.386 | 13 | 0.214 | 5 |
Quanzhou | 0.496 | 8 | 0.388 | 12 | 0.195 | 9 |
Xing’an | 0.558 | 4 | 0.375 | 16 | 0.210 | 6 |
Yongfu | 0.761 | 1 | 0.423 | 5 | 0.321 | 1 |
Guanyang | 0.420 | 11 | 0.368 | 17 | 0.159 | 12 |
Longsheng | 0.317 | 14 | 0.404 | 10 | 0.131 | 15 |
Ziyuan | 0.250 | 16 | 0.376 | 15 | 0.096 | 17 |
Pingle | 0.543 | 5 | 0.400 | 11 | 0.218 | 4 |
Lipu | 0.685 | 2 | 0.406 | 9 | 0.277 | 2 |
Gongcheng | 0.524 | 6 | 0.384 | 14 | 0.204 | 7 |
Whole region | 0.514 | - | 0.395 | - | 0.205 | - |
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Yue, W.; Ren, C.; Liang, Y.; Liang, J.; Lin, X.; Yin, A.; Wei, Z. Assessment of Wildfire Susceptibility and Wildfire Threats to Ecological Environment and Urban Development Based on GIS and Multi-Source Data: A Case Study of Guilin, China. Remote Sens. 2023, 15, 2659. https://doi.org/10.3390/rs15102659
Yue W, Ren C, Liang Y, Liang J, Lin X, Yin A, Wei Z. Assessment of Wildfire Susceptibility and Wildfire Threats to Ecological Environment and Urban Development Based on GIS and Multi-Source Data: A Case Study of Guilin, China. Remote Sensing. 2023; 15(10):2659. https://doi.org/10.3390/rs15102659
Chicago/Turabian StyleYue, Weiting, Chao Ren, Yueji Liang, Jieyu Liang, Xiaoqi Lin, Anchao Yin, and Zhenkui Wei. 2023. "Assessment of Wildfire Susceptibility and Wildfire Threats to Ecological Environment and Urban Development Based on GIS and Multi-Source Data: A Case Study of Guilin, China" Remote Sensing 15, no. 10: 2659. https://doi.org/10.3390/rs15102659
APA StyleYue, W., Ren, C., Liang, Y., Liang, J., Lin, X., Yin, A., & Wei, Z. (2023). Assessment of Wildfire Susceptibility and Wildfire Threats to Ecological Environment and Urban Development Based on GIS and Multi-Source Data: A Case Study of Guilin, China. Remote Sensing, 15(10), 2659. https://doi.org/10.3390/rs15102659